19. Gradients and Ecotones Flashcards
What causes environmental gradients? 2
- physical and chemical properties of water
2. interaction with surrounding environment
what important nutrients my be limiting in freshwaters? 4
- Nitrogen
- Phosphorous
- Silicon
- These influence the biology and chemistry of the freshwater system
Describe the nitrogen cycle in freshwater. 10
- Most nitrogen fixed in soil
- Precipitation of bioavailable N only important in oligotrophic (low nutrient) lakes
- Nitrogen fixation does occur in water
- by cyanobacteria (blue-green algae)
- occurs largely in heterocysts
- generally low but significant in eutrophic lake
- Inorganic nitrogen from
groundwater and surface run-off largely NO3- and NH4+, but amount of NH4+ influenced by pH:
NH4+ ↔ NH4OH - At higher pH, less NH4+
- Inorganic nitrogen is the main form
- ammonium (nh4+) is important in plant biodiversity
Describe the phosphorous cycle in freshwater. 7
- Phosphate (PO4) main source of P to plants
- Largely via erosion of land but tightly bound and so not bioavailable – e.g. Apatite
Ca10(PO4)6(OH,F,Cl,Br)2 - must be broken down - P also adsorbed onto clays and ferric hydroxide
- Both deposited in the sediments therefore major reservoir for P
- Not easily released - non-bioavailable
- Solubility (and hence availability) dependent on conditions in sediments – increased by:
- low dissolved oxygen
- low pH
- Availability comes from soil and run off
How does the presence or absence of oxygen influence the phosphorous cycle? 4
- in anoxic conditions, phsophorous is in form of phosphate
- in oxic conditions, iron is insoluble iron hydroxide thar binds phosphate so low bioavailability
- Diffusion of oxygen low in sediment (max 1-2cm) so release of P inhibited: marked PO4 gradient at sediment/water interface
- Mixing is important to prevent eutrophication in artificial lakes, as disturbance of anoxic sediment releases phosphorous
What factors influence the phosphorous cycle in water? 8
- FALL IN PH
- solubilise apatitie, and so releases PO4
- de-absorbs PO4 due to replacement with H+
- SEDIMENT DISTURBANCE
- anaerobic bacteria – CH3 and H2S
- bioturbation (e.g. chironomid larvae); feeding by fish
- MACROPHYTES
- roots oxygenate sediment and reduce phospherous
What are the characteristics and physical constraints of freshwater systems? 6
- Wetland - land area saturated with water, either permanently or seasonally
- Rivers & streams – running or lotic waters (from L. lavere – to wash)
- Lake/pond - static fresh or salt water in a basin surrounded by land.
- Standing or lentic waters (L. lentus - sluggish)
- Stratification less likely in shallow ponds and lakes (> 5m)
- No agreement on definition of pond:
- light regime: “standing body of water where light penetrates to the bottom”
- size: but no agreement - max area varies from 5 to 8 hectares
Describe deep freshwater lakes - deeper than 5m. 4
- Photic zone: part of water column - where light penetrates
- Distinction between shoreline (littoral) and central zone: macrophytes in photic zone
- In summer, stratified water column differentiated into autotrophic epilimnion and heterotrophic hypolimnion
- Benthic community: macrophytes and algal mats in photic zone; heterotrophic (bacterial-dominated) in aphotic zone
Describe shallow, unstratified lakes and wetlands. 5
- Photic zone: whole of water column
- Distinction between littoral and central zone: macrophytes in both zones
- Depths
Describe an erosional river/stream system. 5
- Photic zone: throughout water column
Distinction between littoral and central zone: little difference - Allochthonous input > autochthonous
- Allochthonous – imported material, e.g. deciduous leaves; autochthonous – produced within the system, e.g. phytoplankton, benthic algae, macrophytes
4.Benthic community: epibenthic algae as high flow prevents rooted macrophytes and phytoplankton - Sediment: course so oxic and hence aerobic heterotrophic community
Describe a depositional river/stream. 6
- Photic zone: throughout water column
- Distinction between littoral (shore) and central zone: pronounced, with emergent macrophytes in littoral zone
- Allochthonous input =/ few mm
Describe the availability of organic matter in the 4 freshwater ecosystems. 4
- Primary production within the system (autochthonous) forms majority of organic matter in standing waters
- Less contribution from littoral zone in upland nutrient-poor standing waters
- Imported organic matter (autochthonous) contributes most in erosional streams and rivers
- Some contribution to autochthonous by plankton in very slow flowing rivers
What is an ecotone? 6
- Zone of transition, and interaction, between adjacent biological systems (from Greek tonos or tension)
- Important in freshwaters
- wide: e.g. wetlands – transition from aquatic to terrestrial
- narrow: stream with bed-rock channel
- often higher biological diversity and density – the edge effect
- edge species – those that use edges for reproduction and survival
What is the ecotone edge affect, and how does this manfiest itself at River Sinnamary? 5
- Higher biological diversity and density – the edge effect
- River Sinnamary, French Guiana - tropical watercourse with number of types of vegetation
3 Edges had highest number of fish species: 46 compared to 24 in channel - due to allochthonous (imported from outside) sources (e.g. leaves, fruit, flowers)
- important to fish populations